Koha online

Geologi dan sumber mineral kawasan Kuala Tembeling, Pahang Darul Makmur (Record no. 868)

000 -LEADER
fixed length control field 02210nam a22001937a 4500
008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
fixed length control field 160218t2012 my 000 0 may|
020 ## - INTERNATIONAL STANDARD BOOK NUMBER
International Standard Book Number 978-967-0159-11-9
082 ## - DEWEY DECIMAL CLASSIFICATION NUMBER
Classification number 555.9 JAS
100 ## - MAIN ENTRY--PERSONAL NAME
Numeration Jasmi bin Ab. Talib
245 ## - TITLE STATEMENT
Title Geologi dan sumber mineral kawasan Kuala Tembeling, Pahang Darul Makmur
250 ## - EDITION STATEMENT
Edition statement Laporan peta 23
260 ## - PUBLICATION, DISTRIBUTION, ETC.
Place of publication, distribution, etc. Kuala Lumpur:
Name of publisher, distributor, etc. Jabatan Mineral dan Geosains Malaysia, Kementerian Sumber Asli dan Alam Sekitar,
Date of publication, distribution, etc. 2012.
300 ## - PHYSICAL DESCRIPTION
Extent i - xi.- 108 p.- ill.- 30.3 cm .-Hard cover.-
Accompanying material Accompanying material: Geological Map (Kuala Tembeling.- New Series L 7010.- Sheet 69.- Scale 1 : 63,360)
500 ## - GENERAL NOTE
General note Price: RM 100.00
942 ## - ADDED ENTRY ELEMENTS (KOHA)
Source of classification or shelving scheme
520 ## - SUMMARY, ETC.
Summary, etc. Abstract.<br/><br/>The study area is located at central Pahang covering the whole topographic map Sheet 69 Kuala Tembeling, Series L 7010 with an area of coverage approximately 1,200 km. It is dominated by low to medium terrain with 60% of the area covered by primary and secondary forest. Six lithostratigraphic units and intrusive rocks had been identified in the study area. The lithostratigraphic units are the Telong Formation., Semantan Formation, Kaling Formation, Kerum Formation, Mangking Sandstone and Termus Shale.<br/><br/>In the study area, the Telong Formation is divisible into two informal members namely the Kayu Ara member and Kenong member. The Kayu Ara member is essentially made up of argillaceous and pyroclastic rocks, whereas the Kenong member consists mainly of calcareous rocks. The Telong Formation was probably deposited during late Middle Permain to Middle Triassic. The age is based on the occurrences of algae, foraminiferas and corals found in the Kenong member.<br/><br/>More than half of this area is covered by the Semantan and Kaling Formations. The Semantan Formation comprises interbedded argillaceous and tuffs whilst the Kaling Formation is composed predominantly of argillaceous, arenaceous and rudaceous rocks. The presence of Posidonia, Daonella, Myophoris and ammonites indicates the age of the Semantan Formation is early Middle Triassic to Late Triassic. <br/><br/> <br/>
648 ## - SUBJECT ADDED ENTRY--CHRONOLOGICAL TERM
General subdivision Geology
Chronological subdivision Malaysia
Geographic subdivision Kuala Tembeling, Pahang
650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM
General subdivision Mineral Resources
Chronological subdivision Malaysia
Geographic subdivision Kuala Tembeling, Pahang
Holdings
Withdrawn status Lost status Source of classification or shelving scheme Damaged status Not for loan Collection code Permanent Location Current Location Shelving location Date acquired Coded location qualifier Cost, normal purchase price Total Checkouts Full call number Date last seen Price effective from Koha item type Copy number Cost, replacement price
Available         Non Fiction BPT BPT General Stacks 02/12/2016 Rak A 100.00   555.951 02/12/2016 02/12/2016 Books    
Available       Staff Collection Map Report and Memo JMG SABAH JMG SABAH Map Report and Memo 24/09/2024   100.00     24/09/2024 24/09/2024 Reference 1 100.00